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Jean-Louis Edouard

Researcher at Aix-Marseille University

Publications -  48
Citations -  1126

Jean-Louis Edouard is an academic researcher from Aix-Marseille University. The author has contributed to research in topics: Holocene & Larch. The author has an hindex of 14, co-authored 47 publications receiving 986 citations. Previous affiliations of Jean-Louis Edouard include Centre national de la recherche scientifique.

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Climate response to the Samalas volcanic eruption in 1257 revealed by proxy records

TL;DR: In this article, the authors used historical archives, ice-core data and tree-ring records to reconstruct the spatial and temporal climate response to the Samalas eruption, finding that 1258 and 1259 experienced some of the coldest Northern Hemisphere summers of the past millennium.
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Blue Reflectance Provides a Surrogate for Latewood Density of High-latitude Pine Tree Rings

TL;DR: In conifers growing at high latitudes and altitudes, the maximum density of tree rings is closely related to climate but is difficult and very expensive to measure as discussed by the authors, which is why it is difficult to measure.

Pine as Climate Indicators in a Dry Subalpine Environment, French Alps

TL;DR: In this article, the authors measured pine latewood width, density, and stable carbon isotope ratios at two sites, separated in altitude by 400 m, close to the forest limit on a south-facing slope in the western French Alps.
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Latewood Width, Maximum Density, and Stable Carbon Isotope Ratios of Pine as Climate Indicators in a Dry Subalpine Environment, French Alps

TL;DR: In this paper, the authors measured pine latewood width, density, and stable carbon isotope ratios at two sites, separated in altitude by 400 m, close to the forest limit on a south-facing slope in the western French Alps.
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Calendar-dated glacier variations in the western European Alps during the Neoglacial: the Mer de Glace record, Mont Blanc massif

TL;DR: In this paper, the first dendrochronologically-based and calendar-dated Neoglacial glacier chronology for the Mont Blanc massif, French Alps is presented. But it is based on the analysis of over 240 glacially buried Pinus cembra subfossil logs and wood remains found either embedded-in-till or as detrital material in the Mer de Glace right lateral moraine.